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The migration ellipse

Another insight into equation (5) is to regard the offset h and the total travel time t as fixed constants. Then the locus of possible reflectors turns out to describe an ellipse in the plane of (y-y0 ,z). The reason it is an ellipse follows from the geometric definition of an ellipse. To draw an ellipse, place a nail or tack into s on Figure 17 and another into g. Connect the tacks by a string that is exactly long enough to go through (y0 ,z). An ellipse going through (y0 ,z) may be constructed by sliding a pencil along the string, keeping the string tight. The string keeps the total distance tv constant.

Recall that one method for migrating zero-offset sections is to take every data value in (y,t)-space and use it to superpose an appropriate semicircle in (y,z)-space. For nonzero offset the circle should be generalized to an ellipse (Figure [*]).

It is not easy to show that equation (5) can be cast in the standard mathematical form of an ellipse, namely, a stretched circle. But the result is a simple one, and an important one for later analysis, so here we go. Equation (5) in (y,h)-space is  
 \begin{displaymath}
t\,v\ \eq \ \sqrt { z^2\ +\ {( y \ -\ y_0 \ - \ h) }^2} 
 \ +\ \sqrt { z^2\ +\ {( y \ -\ y_0 \ + \ h) }^2}\end{displaymath} (9)
To help reduce algebraic verbosity, define a new y equal to the old one shifted by y0. Also make the definitions
            \begin{eqnarray}
t\,v_{\rm rock} \ \ \ \ &=&\ \ \ \ 2\ d\ \eq \ 2\ t\ v_{\rm hal...
 ... z^2 \ \ +\ \ (y\ -\ h)^2
\\ a\ \ -\ \ b\ \ \ \ &=&\ \ \ \ 4\ y\ h\end{eqnarray} (10)
(11)
(12)
(13)
With these definitions, (9) becomes  
 \begin{displaymath}
2\ d\ \eq \ \sqrt a \ \ +\ \ \sqrt b\end{displaymath} (14)
Square to get a new equation with only one square root.  
 \begin{displaymath}
4\ d^2 \ \ -\ \ (a\ +\ b) \ \eq \ 2\ \sqrt a \sqrt b\end{displaymath} (15)
Square again to eliminate the square root.
      \begin{eqnarray}
16\ d^4 \ \ -\ \ 8\ d^2 \, (a\ +\ b) \ \ +\ \ (a\ +\ b)^2 \ \ \...
 ...\ \ 8\ d^2 \, (a\ +\ b) \ \ +\ \ (a\ -\ b)^2 \ \ \ \ &=&
\ \ \ \ 0\end{eqnarray} (16)
(17)
Introduce definitions of a and b.  
 \begin{displaymath}
16\ d^4 \ \ -\ \ 8\ d^2 \ [\,2\,z^2 \ +\ 2\,y^2 \ +\ 2\,h^2 ] \ \ +\ \ 
16\ y^2 \, h^2 \ \eq \ 0\end{displaymath} (18)
Bring y and z to the right.
         \begin{eqnarray}
d^4 \ \ -\ \ d^2 \, h^2 \ \ \ \ &=&\ \ \ \ 
d^2 \, ( z^2 \ +\ y...
 ... \ \ \ \ &=&\ \ \ \ {z^2 \over 1 \ -\ {h^2 \over d^2}}\ \ +\ \ y^2\end{eqnarray} (19)
(20)
(21)
Finally, recalling all earlier definitions,  
 \begin{displaymath}
t^2 \ v_{\rm half}^2 \ \eq \ 
{z^2 \over 1 \ -\ {h^2 \over t^2 \ v_{\rm half}^2}} \ \ +\ \ 
(y\ -\ y_0 )^2\end{displaymath} (22)

Fixing t, equation (22) is the equation for a circle with a stretched z-axis. Our algebra has confirmed that the ``string and tack'' definition of an ellipse matches the ``stretched circle'' definition. An ellipse in model space is the earth model given the observation of an impulse on a constant-offset section.

 
ellipse
ellipse
Figure 23
Migration ellipse.


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shell
shell
Figure 24
Undocumented data from a recruitment brochure. This data may be assumed to be of textbook quality. The speed of sound in water is about 1500 m/sec. Identify the events at A, B, and C. Is this a common-shotpoint gather or a common-midpoint gather? (Shell Oil Company)


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previous up next print clean
Next: SURVEY SINKING WITH THE Up: INTRODUCTION TO DIP Previous: Velocity of sideswipe
Stanford Exploration Project
10/31/1997